Hamidreza Erfani, Reza Haghani, James McClure, Edo Boek, Carl Fredrik Berg
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引用次数: 0
Abstract
Wettability is one of the critical parameters affecting multiphase flow in porous media. The wettability is determined by the affinity of fluids to the rock surface, which varies due to factors such as mineral heterogeneity, roughness, ageing, and pore-space geometry. It is well known that wettability varies spatially in natural rocks, and it is still generally considered a constant parameter in pore-scale simulation studies. The accuracy of pore-scale simulation of multiphase flow in porous media is undermined by such inadequate wettability models. The advent of in situ visualization techniques, e.g. X-ray imaging and microtomography, enables us to characterize the spatial distribution of wetting more accurately. There are several approaches for such characterization. Most include the construction of a meshed surface of the interface surfaces in a segmented X-ray image and are known to have significant errors arising from insufficient resolution and surface-smoothing algorithms. This work presents a novel approach for spatial determination of wetting properties using local lattice-Boltzmann simulations. The scheme is computationally efficient as the segmented X-ray image is divided into subdomains before conducting the lattice-Boltzmann simulations, enabling fast simulations. To test the proposed method, it was applied to two synthetic cases with known wettability and three datasets of imaged fluid distributions. The wettability map was obtained for all samples using local lattice-Boltzmann calculations on trapped ganglia and optimization on surface affinity parameters. The results were quantitatively compared with a previously developed geometrical contact angle determination method. The two synthetic cases were used to validate the results of the developed workflow, as well as to compare the wettability results with the geometrical analysis method. It is shown that the developed workflow accurately characterizes the wetting state in the synthetic porous media with an acceptable uncertainty and is better to capture extreme wetting conditions. For the three datasets of imaged fluid distributions, our results show that the obtained contact angle distributions are consistent with the geometrical method. However, the obtained contact angle distributions tend to have a narrower span and are considered more realistic compared to the geometrical method. Finally, our results show the potential of the proposed scheme to efficiently obtain wettability maps of porous media using X-ray images of multiphase fluid distributions. The developed workflow can help for more accurate characterization of the wettability map in the porous media using limited experimental data, and hence more accurate digital rock analysis of multiphase flow in porous media.
摘要 润湿性是影响多孔介质中多相流的关键参数之一。润湿性由流体与岩石表面的亲和力决定,而岩石表面的亲和力因矿物异质性、粗糙度、老化和孔隙空间几何形状等因素而变化。众所周知,天然岩石的润湿性在空间上是变化的,但在孔隙尺度模拟研究中,润湿性通常仍被视为一个常数。这种不完善的润湿性模型影响了多孔介质中多相流孔隙尺度模拟的准确性。X 射线成像和显微层析成像等原位可视化技术的出现,使我们能够更准确地描述润湿的空间分布特征。这种表征方法有多种。大多数方法包括在分割的 X 射线图像中构建界面表面的网格面,众所周知,由于分辨率和表面平滑算法不足,这种方法存在很大误差。这项研究提出了一种利用局部晶格-玻尔兹曼模拟空间确定润湿特性的新方法。该方案计算效率高,因为在进行晶格-玻尔兹曼模拟之前,已将分割的 X 射线图像划分为多个子域,从而实现了快速模拟。为了测试所提出的方法,我们将其应用于两个已知润湿性的合成案例和三个成像流体分布数据集。通过对被困神经节的局部晶格-玻尔兹曼计算和表面亲和力参数的优化,获得了所有样本的润湿性图。结果与之前开发的几何接触角测定方法进行了定量比较。利用两个合成案例验证了所开发工作流程的结果,并将润湿性结果与几何分析方法进行了比较。结果表明,所开发的工作流程能准确描述合成多孔介质的润湿状态,其不确定性在可接受范围内,而且能更好地捕捉极端润湿条件。对于三个成像流体分布数据集,我们的结果表明所获得的接触角分布与几何分析方法一致。不过,与几何方法相比,所获得的接触角分布往往跨度较窄,被认为更符合实际情况。最后,我们的研究结果表明,所提出的方案具有利用多相流体分布的 X 射线图像高效获取多孔介质润湿性图的潜力。开发的工作流程有助于利用有限的实验数据更准确地描述多孔介质中的润湿性图,从而更准确地对多孔介质中的多相流进行数字岩石分析。
期刊介绍:
-Publishes original research on physical, chemical, and biological aspects of transport in porous media-
Papers on porous media research may originate in various areas of physics, chemistry, biology, natural or materials science, and engineering (chemical, civil, agricultural, petroleum, environmental, electrical, and mechanical engineering)-
Emphasizes theory, (numerical) modelling, laboratory work, and non-routine applications-
Publishes work of a fundamental nature, of interest to a wide readership, that provides novel insight into porous media processes-
Expanded in 2007 from 12 to 15 issues per year.
Transport in Porous Media publishes original research on physical and chemical aspects of transport phenomena in rigid and deformable porous media. These phenomena, occurring in single and multiphase flow in porous domains, can be governed by extensive quantities such as mass of a fluid phase, mass of component of a phase, momentum, or energy. Moreover, porous medium deformations can be induced by the transport phenomena, by chemical and electro-chemical activities such as swelling, or by external loading through forces and displacements. These porous media phenomena may be studied by researchers from various areas of physics, chemistry, biology, natural or materials science, and engineering (chemical, civil, agricultural, petroleum, environmental, electrical, and mechanical engineering).